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Calcite-dolomite thermometry: Negative evidence from the Marmorilik Formation, West Greenland (1977)

Garde, Adam A.

Springer

Contributions to mineralogy and petrology 62 (1977), S. 265-270

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ISSN: 1432-0967

Source: Springer Online Journal Archives 1860-2000

Topics: Geosciences

Notes: Abstract Calcite grains from 19 composite dolomite-calcite marble samples from the Marmorilik Formation, West Greenland, have been analysed for Ca, Mg, and Fe with the microprobe in order to estimate metamorphic temperatures using the calcite-dolomite solvus geothermometer. The results show that there are large variations within single samples, and, insofar as any thermal gradient can be detected, it is the opposite of that indicated by mineral parageneses. Current practice in the application of the method is therefore questioned.

Type of Medium: Electronic Resource

URL: http://dx.doi.org/10.1007/BF00371014

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